To create the seabed forms layer, the Benthic Position Index (BPI) was calculated using a regional bathymetry layer as input. NOAA’s Benthic Terrain Modeler was used for these calculations. BPI was calculated at two separate scales:
“Broad-scale” BPI - inner radius: 9 cells; outer radius: 90 cells, standardized
“Fine-scale” BPI - inner radius: 3 cells; outer radius: 25 cells, standardized
The resulting layers were then reclassified to determine the “features” at both scales. Four classes were created to visualize Broad-scale features: Deep valley, Valley, Peak, and High-peak. For fine-scale features, there are two classes: deep valleys and high peaks. The two resulting layers were them combined to create the final seabed forms.